B
Bruno Lanson
Researcher at University of Savoy
Publications - 121
Citations - 8145
Bruno Lanson is an academic researcher from University of Savoy. The author has contributed to research in topics: Illite & Birnessite. The author has an hindex of 47, co-authored 112 publications receiving 7241 citations. Previous affiliations of Bruno Lanson include École Normale Supérieure & Joseph Fourier University.
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Structure of heavy-metal sorbed birnessite: Part 1. Results from X-ray diffraction
Bruno Lanson,Victor A. Drits,Victor A. Drits,Anne-Claire Gaillot,Ewen Silvester,Ewen Silvester,A. Plançon,Alain Manceau +7 more
TL;DR: In this paper, selected-area electron diffraction (SAED) and energy dispersive analysis were used to study the structure of synthetic heavy-metal sorbed birnessites (MeBi), including Pb, Cd, Zn, and Cu.
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Structure of nanocrystalline phyllomanganates produced by freshwater fungi
TL;DR: The crystal structures of biogenic Mn oxides produced by three fungal strains isolated from stream pebbles were determined using chemical analyses, XANES and EXAFS spectroscopy, and powder X-ray diffraction as discussed by the authors.
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Hydration Properties and Interlayer Organization of Water and Ions in Synthetic Na-Smectite with Tetrahedral Layer Charge. Part 2. Toward a Precise Coupling between Molecular Simulations and Diffraction Data
Eric Ferrage,Boris A. Sakharov,Laurent J. Michot,Alfred Delville,Allan Bauer,Bruno Lanson,Sylvain Grangeon,Gilles Frapper,Mónica Jiménez-Ruiz,Gabriel J. Cuello +9 more
TL;DR: Cygan et al. as mentioned in this paper developed a specific methodology to collate the interlayer configurations resulting from Grand-Canonical Monte Carlo (GCMC) simulations with experimental X-ray and neutron diffraction data for two synthetic Na-saturated saponites having contrasting layer charge.
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Characterization of the End of Smectite-to-Illite Transformation: Decomposition of X-Ray Patterns
Bruno Lanson,Gerard Besson +1 more
TL;DR: In this article, a simulation-decomposition approach for modeling X-ray diffraction (XRD) patterns is introduced to describe quickly and accurately the various clay minerals (essentially mixed-layer illite/smectite and illite) present in a sedimentary series, and to follow their individual evolution during diagenesis.
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EXPERIMENTAL INVESTIGATION OF THE INTERACTION OF CLAYS WITH HIGH-pH SOLUTIONS: A CASE STUDY FROM THE CALLOVO-OXFORDIAN FORMATION, MEUSE-HAUTE MARNE UNDERGROUND LABORATORY (FRANCE)
TL;DR: In this article, the impact of alkaline solutions on the clay mineralogy of the Callovo-Oxfordian formation hosting the French underground laboratory for nuclear waste disposal investigation (Meuse- Haute Marne site) has been studied experimentally.